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Hutton, James, 1726-1797

"Theory of the Earth, Volume 1 (of 4)"


Thus, we have sufficient reason to believe, that, in knowing the
construction of the land in Europe, we know the constitution of the land
in every part of the globe. Therefore, we may proceed to form general
conclusions, from the knowledge of the mineral region, thus acquired in
studying those parts which are seen.
Having thus found, _first_, That the consolidated and indurated masses
of our strata had suffered the effects of violent heat and fusion;
_2dly_, That those strata, which had been formed in a regular manner at
the bottom of the sea, have been violently bended, broken, and removed
from their original place and situation; and, _lastly_, Having now found
the most indubitable proof, that the melting, breaking, and removing
power of subterraneous fire, has been actually exerted upon this land
which we examine, we cannot hesitate in ascribing these operations as a
cause to those effects which are exposed to our view. Now, these may be
considered as consisting in the solid state and present situation of
those stratified bodies, originally formed by subsidence in the ocean;
appearances which cannot, in reason, be ascribed to any other cause, and
which, upon this principle, are perfectly explained.


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